distanta rutiera caransebes sibiu 100

Their high mineralization predominantly sodium salts led to both the salinization and sodization of the horizons located above the aquifer. The dispersion of torrential basins and the high density of gullies and furrows within the sub-basins of the Bistra, Dobra, Purcariul, Martinie, Dumbrava, Valea Caselor and the ravine character of the springs from the hills near the mountains Calnic, Garbova, Reciu and the plateau Daia, Boz, Sangatin, Gusu causes a spasmodic drainage regime, which in case of abundant precipitation may lead to disequilibria. The grey sandy soil layer, which is cm thick, covers a deposit of yellowish sand that is very fine, silty, micaceous, with more clayish and darker lens. No added fees. For exemple, the lowest monthly means correspond to

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